Investigate the movement of water into and out of plant cells by osmosis.

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Potato Cores in Salt Solution

Scenario

Plants in the soil have their roots in a dilute solution of mineral ions. When they are suddenly

flooded with seawater, concentration of which is 0.3 molar Sodium Chloride, they are observed

to wilt and become flaccid.

Aim

The aim of this experiment is to investigate the movement of water into and out of plant cells by

osmosis. The cells chosen for study will be taken from potato tubers as they provide a ready

supply of uniform material.

Background Information

Any substance dissolved in water is called a solute; a solvent is a liquid that is able to dissolve

another substance, called a solute, to form a solution.

The water content of plants varies depending on environmental conditions. In land plants it plays

a vital role in structural support and mineral transport and thus a lack of water may lead to

wilting or possibly death.

Water is mainly absorbed through the roots, which are covered in specially adapted root hair

cells, with large surface areas and thin cell walls to aid absorption by osmosis. The evaporation

of water through stomata on plant leaves causes a transpiration stream, causing the water to be

drawn up through xylem vessels.

Osmosis is the flow of water molecules by diffusion through a partially permeable membrane

from areas of high water potential (low solute concentrations) to regions of low water potential

(high solute concentrations).

All plant cell membranes are partially permeable, which means they allow some some

substances to penetrate them but not others.

Whether water enters the cell by osmosis will depend on the balance between external and

internal solute and water potentials. If the solutions on each side of the partially permeable

membrane are of equal water or solute potential, then there will be no net movement of water

molecules across the membrane. This is called an equilibrium state and the solutions are referred

to as being isotonic.

A solution that contains more solute particles than another, and hence has a low water potential,

is referred to as being hypertonic, whilst the less concentrated solution is hypotonic.

The concentration of solute particles is described as a molarity. One mole of any substance is

the mass of 6.02 x 1023 particles of the substance. The molarity of a solution can be calculated

using the below equation:

Molarity = Moles of Solute

Litres of Solution

If a plant was exposed to a waterlogged environment, with the external solute concentration to

the cell being hypotonic to the vacuole contents, the cell will not continue to take in water by

osmosis forever. The cellulose wall provides a rigid barrier to uncontrolled expansion. A cell

that is full of water is called turgid and cannot expand further as the inward force of the starched

wall balances the outward pressure on the cell contents. This wall pressure is called turgor

pressure and the internal outward force on the wall is called the osmotic pressure.

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At the other extreme, a cell placed in a solution that is hypertonic to its contents will lose water

molecules by osmosis. The cytoplasm will cease to exert a pressure on the cellulose cell wall

and the cell, described as flaccid, will lack support. Water loss can continue to such an extent

that the cytoplasm, and attached cell membrane, contracts and detaches from the cell wall. A

cell in this condition is said to be plasmolysed and this damage is irreversible.

Safety notes

· Use care when working with glassware.

· Wash your ...

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